Adaptively constraining radar attenuation and temperature across the Thwaites Glacier catchment using bed echoes
Englacial temperature is a major control on ice rheology and flow. However, it is difficult to measure at the glacier to ice-sheet scale. As a result, ice-sheet models must make assumptions about englacial temperature and rheology, which affect sea level projections. This is problematic if fundament...
| Published in: | Journal of Glaciology |
|---|---|
| Main Authors: | , , , |
| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
Cambridge University Press
2016
|
| Subjects: | |
| Online Access: | https://doi.org/10.1017/jog.2016.100 https://doaj.org/article/2212a5e66b954740a0daa8aa054a37f7 |